Mitrofanovite
A valid IMA mineral species
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Formula:
Pt3Te4
Lustre:
Metallic
Crystal System:
Trigonal
Name:
Named in honour Felix Petrovich Mitrofanov (Феликс Петрович Митрофанов) (22 June 1935, Orenburg, USSR - 8 May 2014, Apatity, Russia), geologist and Academician of the Russian Academy of Science. He was among the first to discover platinum-group mineralization in the Fedorova-Pana complex, Russia.
Unique Identifiers
Mindat ID:
52901
Long-form identifier:
mindat:1:1:52901:5
GUID
(UUID V4):
(UUID V4):
21a37e63-7e3e-4ad3-9be3-807b7229a7fd
IMA Classification of Mitrofanovite
Approved
Approval year:
2018
First published:
2019
Classification of Mitrofanovite
1.AH.
1 : ELEMENTS (Metals and intermetallic alloys; metalloids and nonmetals; carbides, silicides, nitrides, phosphides)
A : Metals and Intermetallic Alloys
H : Miscellaneous Elements, alloys
1 : ELEMENTS (Metals and intermetallic alloys; metalloids and nonmetals; carbides, silicides, nitrides, phosphides)
A : Metals and Intermetallic Alloys
H : Miscellaneous Elements, alloys
Mineral Symbols
As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.
Symbol | Source | Reference |
---|---|---|
Mfv | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Physical Properties of Mitrofanovite
Optical Data of Mitrofanovite
Anisotropism:
Strong, greyish brown rotation tints
Bireflectance:
medium to strong
Reflectivity:
Wavelength | R1 | R2 |
---|---|---|
470nm | 58.4% | 54.6% |
546nm | 62.7% | 58.0% |
589nm | 63.4% | 59.1% |
650nm | 63.6% | 59.5% |
Graph shows reflectance levels at different wavelengths (in nm). Top of box is 100%. Peak reflectance is 63.6%.
R1 shown in black, R2 shown in red
Colour in reflected light:
bright white
Internal Reflections:
None
Pleochroism:
Weak
Chemistry of Mitrofanovite
Mindat Formula:
Pt3Te4
Elements listed:
Crystallography of Mitrofanovite
Crystal System:
Trigonal
Class (H-M):
3m - Ditrigonal Pyramidal
Space Group:
R3m
Cell Parameters:
a = 3.9875(1) Å, c = 35.362(7) Å
Ratio:
a:c = 1 : 8.868
Unit Cell V:
486.93 ų (Calculated from Unit Cell)
X-Ray Powder Diffraction
Powder Diffraction Data:
d-spacing | Intensity |
---|---|
11.79 Å | (23) |
5.891 Å | (100) |
3.928 Å | (11) |
2.851 Å | (26) |
2.137 Å | (16) |
2.039 Å | (18) |
1.574 Å | (24) |
1.310 Å | (21) |
Comments:
From Type Description.
Geological Environment
Paragenetic Mode(s):
Paragenetic Mode | Earliest Age (Ga) |
---|---|
Stage 4b: Highly evolved igneous rocks | >3.0 |
37 : Layered igneous intrusions and related PGE minerals |
Type Occurrence of Mitrofanovite
General Appearance of Type Material:
Anhedral grains (up to about 20×50μm) commonly in intergrowths with moncheite
Place of Conservation of Type Material:
Type material is deposited in the collections of the Fersman Mineralogical Museum, Russian Academy of Sciences, Moscow, Russia, registration number 5141/1
Geological Setting of Type Material:
Low-sulphide disseminated ore
Associated Minerals at Type Locality:
Reference:
Subbotin, V.V., Vymazalová, A., Laufek, F., Savchenko, Y.E., Stanley, C.J., Gabov, D.A., Plášil, J. (2019) Mitrofanovite, Pt3Te4, a new mineral from the East Chuarvy deposit, Fedorovo–Pana intrusion, Kola Peninsula, Russia. Mineralogical Magazine: 83(4): 523-530.
Synonyms of Mitrofanovite
Related Minerals - Strunz-mindat Grouping
1.AH. | Decagonite | Al71Ni24Fe5 |
1.AH. | Orthocuproplatinum | Pt3Cu |
1.AH. | Tomamaeite | Cu3Pt |
1.AH.10 | Cerium | Ce |
1.AH.15 | Tantalum | Ta |
Other Information
Health Risks:
No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.
Internet Links for Mitrofanovite
mindat.org URL:
https://www.mindat.org/min-52901.html
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References for Mitrofanovite
Localities for Mitrofanovite
Locality List
- This locality has map coordinates listed.
- This locality has estimated coordinates.
ⓘ - Click for references and further information on this occurrence.
? - Indicates mineral may be doubtful at this locality.
- Good crystals or important locality for species.
- World class for species or very significant.
(TL) - Type Locality for a valid mineral species.
(FRL) - First Recorded Locality for everything else (eg varieties).
Struck out - Mineral was erroneously reported from this locality.
Faded * - Never found at this locality but inferred to have existed at some point in the past (e.g. from pseudomorphs).
All localities listed without proper references should be considered as questionable.
All localities listed without proper references should be considered as questionable.
Russia (TL) | |
| Subbotin et al. (2019) |